Forrest (Barney) G Poole (Former Employee)
Science and Products
Filter Total Items: 53
Thermal history and organic maturation of Paleozoic rocks, Pocatello area, southeastern Idaho
No abstract available.
Authors
G. A. Desborough, Forrest G. Poole, A. J. L. Harris, T.A. Daws
Mineral resources of the Goshute Canyon Wilderness Study Area, Elko and White Pine counties, Nevada
No abstract available.
Authors
Forrest G. Poole, Maya Elrick, R. K. Tucker, Reid N. Harris, H. W. Oliver, F. L. Johnson
Mineral Resources of the Antelope Wilderness Study Area, Nye County, Nevada
At the request of the U.S. Bureau of land Management, 83,100 acres of the Antelope Wilderness Study Area (NV-4)60-231/241) was studied. In this report the studied area is called the 'wilderness study area', or simply the 'study area.' No identified mineral or energy resources occur within the study area. The southern part of the area has moderate mineral resource potential for...
Authors
Richard F. Hardyman, Forrest G. Poole, Frank Joseph Kleinhampl, Robert M. Turner, Donald Plouff, Joe S. Duval, Fredrick L. Johnson, David A. Benjamin
Middle Devonian to Late Mississippian event stratigraphy of Overthrust belt region, western United States
Twenty eustatic and epeirogenic events mainly dated by conodonts are distinguished between the Middle Devonian and the lower Upper Mississippian in Great Basin, in Rocky Mountains and in the Overthrust belt regions.
Authors
Charles Sandberg, Raymond C. Gutschick, J.G. Johnson, Forrest G. Poole, W.J. Sando
Metalliferous oil shales in central Montana and northeastern Nevada
No abstract available.
Authors
George A. Desborough, Forrest G. Poole, Gregory N. Green
Quantitative analysis versus semiquantitative optical emission spectrographic analysis of chromium, nickel, zinc, vanadium, and molybdenum in organic-rich Paleozoic marine strata, Western United States
Comparison of analytical results between the quantitative method and the semiquantitative six-step optical-emission spectrographic method commonly shows significantly lower values for the semiquantitative method. The lower values are most obvious for splits from the same samples of fine-grained organic-rich rocks where the concentrations of the metals chromium, nickel, zinc, vanadium...
Authors
George A. Desborough, Forrest G. Poole, Edwin K. Maughan, H.L. Groves, Gregory N. Green
Science and Products
Filter Total Items: 53
Thermal history and organic maturation of Paleozoic rocks, Pocatello area, southeastern Idaho
No abstract available.
Authors
G. A. Desborough, Forrest G. Poole, A. J. L. Harris, T.A. Daws
Mineral resources of the Goshute Canyon Wilderness Study Area, Elko and White Pine counties, Nevada
No abstract available.
Authors
Forrest G. Poole, Maya Elrick, R. K. Tucker, Reid N. Harris, H. W. Oliver, F. L. Johnson
Mineral Resources of the Antelope Wilderness Study Area, Nye County, Nevada
At the request of the U.S. Bureau of land Management, 83,100 acres of the Antelope Wilderness Study Area (NV-4)60-231/241) was studied. In this report the studied area is called the 'wilderness study area', or simply the 'study area.' No identified mineral or energy resources occur within the study area. The southern part of the area has moderate mineral resource potential for...
Authors
Richard F. Hardyman, Forrest G. Poole, Frank Joseph Kleinhampl, Robert M. Turner, Donald Plouff, Joe S. Duval, Fredrick L. Johnson, David A. Benjamin
Middle Devonian to Late Mississippian event stratigraphy of Overthrust belt region, western United States
Twenty eustatic and epeirogenic events mainly dated by conodonts are distinguished between the Middle Devonian and the lower Upper Mississippian in Great Basin, in Rocky Mountains and in the Overthrust belt regions.
Authors
Charles Sandberg, Raymond C. Gutschick, J.G. Johnson, Forrest G. Poole, W.J. Sando
Metalliferous oil shales in central Montana and northeastern Nevada
No abstract available.
Authors
George A. Desborough, Forrest G. Poole, Gregory N. Green
Quantitative analysis versus semiquantitative optical emission spectrographic analysis of chromium, nickel, zinc, vanadium, and molybdenum in organic-rich Paleozoic marine strata, Western United States
Comparison of analytical results between the quantitative method and the semiquantitative six-step optical-emission spectrographic method commonly shows significantly lower values for the semiquantitative method. The lower values are most obvious for splits from the same samples of fine-grained organic-rich rocks where the concentrations of the metals chromium, nickel, zinc, vanadium...
Authors
George A. Desborough, Forrest G. Poole, Edwin K. Maughan, H.L. Groves, Gregory N. Green